Reference soil Kenya 13: Solonetz

KE013

Solonetzes occur where a sodium source supplies the clay-rich subsoil with exchangeable Na, causing peptization of clay and organic substances and deterioration of the topsoil.

Characteristics

Soils having a natric horizon (a subsurface horizon with distinct higher clay content than the overlying horizon and more than 15% exchangeable sodium) within 100 cm from the soil surface.

Distribution of Solonetz (rough estimation supplied by soilgrids)

 

Reference soil KE013: Solonetz

A moderately well drained brown to yellowish brown soil with a moderately sodic subsoil and moderate surface sealing (3mm), derived from fine-grained sandstones and siltstones (Upper Maji-Ya-Chumvi beds). Below 35 cm mottles appear coloured strong brown, increasing with depth; termite mounds (4-7m diameter, 1,5 m height) exist. (R3 pg 253)

 

Classification

WRB 2006WRB 1998
Stagnic- Solonetz (Albic Abruptic Magnesic)Stagni-Mazic- Solonetz (Albic)
20-65 cmalbic horizon
65-120 cmnatric horizon
-reducing conditions
-abrupt textural change
-stagnic colour pattern
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Stagnic SolonetzSolodic Planosol
0-20 cmochric A horizon
20-65 cmalbic E horizon
65-120 cmnatric B horizon
-abrupt textural change
-stagnic
0-20 cmochric A horizon
20-65 cmalbic E horizon
65-120 cmnatric B horizon
-abrupt textural change